Supported by the National Natural Science Foundation of China(42272110);CNPC-China University of Petroleum(Beijing)Strategic Cooperation Project(ZLZX2020-02).
Aiming at the problem that the data-driven automatic correlation methods which are difficult to adapt to the automatic correlation of oil-bearing strata with large changes in lateral sedimentary facies and strata thic...
This perspective is written through the lens of someone who,except for a limited but enlightening foray into the region 25 years ago,has largely watched the evolution of thinking and understanding of the Altaids from ...
financially supported by the National Natural Science Foundation of China(42130305 and 42002227);project of the China Geological Survey(DD20190039-04,DD20179402,DD20190360 and DD20221632);National Key R&D Program of China(2017YFC0601300 and 2013CB429802);Taishan Scholars(ts20190918);Qingdao Leading Innovation Talents(19-3-2-19-zhc).
The eastern Central Asian Orogenic Belt(CAOB)in NE China is a key area for investigating continental growth.However,the complexity of its Paleozoic geological history has meant that the tectonic development of this be...
support from Australian Research Council grant FL160100168;supported by the National Institute of Science and Technology for Tectonic Studies(INCT)of Brazil。
The Alto MoxotóTerrane of the Borborema Province presents a wide exposure of Paleoproterozoic crust,but unlike other continental blocks of South America,its orogenic history is strongly obliterated by late Neoprotero...
the Brazilian National Council for Scientific and Technological Development (CNPq) (309712/2017-30);Brazilian Coordination for the Improvement of Higher Level Personnel (CAPES) (88881.188918/2018-01);Brazilian National Council for Scientific and Technological Development (CNPq Process #404767/2016-8);São Paulo Research Foundation (FAPESP Process #2021/00967-5)
The geometry and evolution of pre-existing basement in accretionary belts bordering supercontinents are often unclear.Integrative interpretation of long-wavelength potential field satellite data can image deep crust s...
the Laboratory for Marine Mineral Resources,Qingdao National Laboratory for Marine Science and Technology(No.MMRKF201810);the China Geological Survey(Nos.DD20190582,DD20191009,DD20160214);funded by the Shandong Province"Taishan Scholar"Construction Project。
To investigate the nature of gas hydrates in the Makran area,new high-resolution geophysical data were acquired between 2018-2019.The data collected comprise multibeam and two-dimensional multi-channel seismic reflect...
The Egyptian Nubian Shield(ENS)represents the northwestern part of the Arabian-Nubian Shield and the northern extension of the East African Orogen.The ENS is regarded as being formed due to northward-directed escape t...
performed within the framework of the IGC State Assignment Project No.0350-2016-0028;Ministry of Science and Technology of Taiwan(MOST 106-2811-M-001-035)during postdoctoral research of SYuS at Institute of Earth Science(Academia Sinica,Taipei,Taiwan);further supported by the Foundation of Russian Federation President(Grant No.MK-67.2020.5)。
In continental subduction complexes minor volumes of high-pressure mafic rocks(eclogites)often co-exist with much more abundant felsic(granitic)and metasedimentary rocks,which are vital for resolving the origin and me...
the National Natural Science Foundation of China(Grant No.41730210);the National Key Research and Development Program of China(Grant No.2017YFC0601304);the Chinese Geological Survey(Grant No.DD20190010);Taishan Scholar Special Project Funds(Grant No.ts201511076).
Accretionary complex was usually formed by offscraping of the subducting crustal material over the trench and thus often referred to as subduction zone mélange.The structure,composition and forming process of accreti...
the RF state project(No.0135-2019-0036);partly supported by the project(No.0135-20180039)of the Program of the Presidium of the RAS“Fundamental problems of geological and geophysical study of lithospheric processes”;the Russian Foundation for Basic Research for supporting project(No.19-05-00336)。
A 3D model of deep crustal structure of the Archaean Karelia Craton and late Palaeoproterozoic Svecofennian Accretionary Orogen including the boundary zone is presented.The model is based on the combination of data fr...